[1] Puthezhath AS. Identification of thermal fronts in the Arabian Sea using MODIS-SST Data [Dissertation]. Kerala university of fisheries and ocean studies; 2014.
[2] Sikhakolli R, Sharma R, Basu S, Gohil BS, Sarkar A, Prasad KV. Evaluation of OSCAR ocean surface current product in the tropical Indian Ocean using in situ data. Journal of earth system science. 2013 Feb 1;122(1):187-99.
[3] Bansal S, Sasamal SK, Rao KH, Dutt CBS. Indian Ocean Surface Current Using OSCAT and Saral-Altika. Hyderabad: Ocean Sciences Group, ECSA, NRSC; 2014.
[4] Shinoda T, Jensen T, Flatau M, Chen S, Han W, Wang C. Large-scale oceanic variability associated with the Madden-Julian oscillation during the CINDY/DYNAMO field campaign from satellite observations. Remote Sensing. 2013 May;5(5):2072-92.
[5] Sanchez-Reales JM, Vigo MI, Jin S, Cha B F.Global Surface Geostrophic Ocean Currents Derived From Satellite Altimetry And GOCE Geoid. Marine Geodesy. 2012; 35(S1):175–89.
[6] Shenoi SS, Saji PK, Almeida AM. Near-surface circulation and kinetic energy in the tropical Indian Ocean derived from Lagrangian drifters. Journal of Marine Research. 1999 Nov 1;57(6):885-907.
[7] Wyrtki K. An Equatorial Jet inthe Indian Ocean. Science. 1976;181: 262–64.
[8] Lecture 8b, INCOIS, Hyderabad. Eddies and Frontal Systems Course on Modeling Indian Ocean Processes and Phenomena. 2015.
[9] Lagerloef GS, Mitchum GT, Lukas RB, Niiler PP. Tropical Pacific near‐surface currents estimated from altimeter, wind, and drifter data. Journal of Geophysical Research: Oceans. 1999 Oct 15;104(C10):23313-26.
[10] Alvarez A, Chiggiato J, Schroeder K. Mapping sub-surface geostrophic currents from altimetry and a fleet of gliders. Deep Sea Research Part I: Oceanographic Research Papers. 2013; Apr 1;74:115-29.